地学前缘 ›› 2021, Vol. 28 ›› Issue (5): 380-412.DOI: 10.13745/j.esf.sf.2020.12.9

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西大别桥店花岗斑岩脉的形成时代、岩石成因及其大地构造意义

黄海永1,2,3(), 徐扬1,2,4,*(), 尹须伟1,3, 杨坤光4, 刘雨4   

  1. 1.中国地质调查局 武汉地质调查中心, 湖北 武汉 430205
    2.中国科学院 广州地球化学研究所 同位素地球化学国家重点实验室, 广东 广州 510640
    3.中国地质大学(北京) 地球科学与资源学院, 北京 100083
    4.中国地质大学(武汉) 构造与油气资源教育部重点实验室, 湖北 武汉 430074
  • 收稿日期:2020-04-10 修回日期:2020-09-01 出版日期:2021-09-25 发布日期:2021-10-30
  • 通讯作者: 徐扬
  • 作者简介:黄海永(1996—),男,硕士研究生,矿物学、岩石学、矿床学专业。E-mail: huanghaiyong96@163.com
  • 基金资助:
    同位素地球化学国家重点实验室(中国科学院广州地球化学研究所)开放-合作基金项目(SKLabIG-KF-18-13);湖北省自然科学基金项目(2020CFB344);中国地质大学(武汉)构造与油气资源教育部重点实验室开放基金项目(TPR-2019-07);中国地质调查局项目(DD20190050)

Geochronology, petrogenesis and tectonic implications of the Qiaodian granite porphyry from the western Dabie Orogenic Belt, Central China

HUANG Haiyong1,2,3(), XU Yang1,2,4,*(), YIN Xuwei1,3, YANG Kunguang4, LIU Yu4   

  1. 1. Wuhan Center, China Geological Survey, Wuhan 430205, China
    2. State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
    3. School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China
    4. Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences(Wuhan),Wuhan 430074, China
  • Received:2020-04-10 Revised:2020-09-01 Online:2021-09-25 Published:2021-10-30
  • Contact: XU Yang

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摘要：

白垩纪碰撞后花岗岩是研究大别造山带碰撞后伸展垮塌的重要载体,西大别南缘的桥店花岗斑岩脉为约束大别山碰撞后构造机制转化提供了新的约束信息。SIMS和LA-ICP-MS锆石定年结果表明,桥店花岗斑岩脉侵位年龄约为129 Ma,并具有富集的锆石Hf同位素组成(εHf(t)=-24.5-14.7)和古元古代二阶段模式年龄(2.41.9 Ga)。矿物组成上,花岗斑岩脉以富含粗粒的长石斑晶为主要特征。它们具有变化的SiO2含量(63.07%73.22%)和A/CNK值(0.871.73),同时具有高的K2O(4.51%5.47%)、低的MgO (0.42%1.82%)含量,属于高钾钙碱性花岗岩类。岩石的轻稀土元素相对重稀土元素富集,具有Eu的负异常(Eu/Eu*=0.770.92);同时富集Rb、Ba和Pb,而亏损Nb、Ta和Ti。相较于典型埃达克质岩石,桥店花岗斑岩的Sr含量(78×10-6724 ×10 -6)变化较大,Y(11.8×10-614.8×10-6)和Yb(1.09×10-61.37×10-6)含量相对较高,对应的Sr/Y(6.755.5)和(La/Yb)N(29.634.2)比值较低。以上地球化学特征,结合古元古代的残留锆石和二阶段铪模式年龄,共同反映出桥店花岗斑岩是区内古元古代下地壳物质在中-低压力条件下部分熔融的产物。与区域上碰撞后岩浆岩的对比研究表明,桥店花岗斑岩的侵位指示了西大别地壳在约129 Ma已经开始减薄,西大别白垩纪加厚下地壳的拆沉及构造机制转换的时间可能在约130 Ma前后。

关键词: 锆石U-Pb-Hf同位素, 高钾钙碱性花岗岩, 早白垩世, 西大别造山带

Abstract:

The ca. 145-120 Ma granitoids were regarded as important products of the thickened, delaminated partial melting Cretaceous crust beneath the Dabie Orogenic Belt. Our newly identified Qiaodian granite porphyry in the western Dabie Orogenic Belt can provide new constraints on the progression of lithospheric thinning and the transformation of tectonic regime to an extensional setting. SIMS and LA-ICP-MS zircon U-Pb dating suggests the Qiaodian granite porphyry was emplaced at 129 Ma. It has a negative zircon εHf(t) value (between -24.5 and -14.7) with a two-stage model age of 2.4-1.9 Ga, and is characterized by coarse-grained feldspar phenocrysts. It has variable SiO2 contents (63.07%-73.22%) and A/CNK values (0.87-1.73), with high K2O(4.51%-5.47%) and low MgO(0.42%-1.82%) contents, suggesting high-K calc-alkaline granite affinity. It exhibits LREE-enriched rare earth elemental distribution patterns ((La/Yb)N=29.6-34.2) with negative Eu anomalies ((Eu/Eu *)=0.77-0.92). The primitive mantle-normalized trace element patterns show enrichments of Rb, Ba and Pb and depletions of Nb, Ta and Ti. Compared with typical adakites, the Qiaodian granite porphyry has variable Sr((78-724)×10-6) and relatively high Y((11.8-14.8)×10-6) and Yb((1.09-1.37)×10-6) contents, yielding a low Sr/Y ratio (6.7-55.5). These geochemical features, together with Paleoproterozoic residual zircon and two-stage Hf model ages, indicate the Qiaodian granite porphyry mainly derived from partial melting of Paleoproterozoic mafic materials at medium to low pressures. On the basis of our new results and previously published data, we consider the tectonic collapse and transformation of the western Dabie Orogenic Belt probably occurred around 130 Ma.

Key words: zircon U-Pb-Hf isotopes, high-K calc-alkaline granite, Early Cretaceous, western Dabie Orogenic Belt

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